Rock Identifier
Possible shale or slate fragment (Fine-grained clay-rich rock; possibly slate (low-grade metamorphosed shale)) — metamorphic
metamorphic

Possible shale or slate fragment

Fine-grained clay-rich rock; possibly slate (low-grade metamorphosed shale)

AI-generated identification · may be incorrect

Small dark gray, thin, angular fragment with dull to slightly silky luster and apparent planar splitting. Likely hardness about 2–4 Mohs; composition may include clay minerals, mica, quartz, and feldspar.

Identified More metamorphic
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Physical properties

Small dark gray, thin, angular fragment with dull to slightly silky luster and apparent planar splitting. Likely hardness about 2–4 Mohs; composition may include clay minerals, mica, quartz, and feldspar.

Formation & geological history

Shale forms from compacted mud in sedimentary basins; slate forms when shale is weakly metamorphosed during burial and tectonic compression, commonly millions to hundreds of millions of years ago.

Uses & applications

Slate is used for roofing, flooring, writing boards, and landscaping; ordinary shale fragments have little commercial value except as aggregate or raw material for cement and bricks.

Geological facts

The image is too small and lacks a fresh surface for confident identification; it could also be a piece of weathered dark stone or construction debris.

Field identification & locations

Look for consistent fine layering, very smooth planar cleavage, and a powdery streak; slate typically splits into thin, flat sheets, while shale feels softer and flakes irregularly. Common worldwide in sedimentary and metamorphic terrains.